Aerosols over continental Portugal (1978–1993): their sources and an impact on the regional climate

Morozova, A. L.; Mironova, I. A.

doi:https://doi.org/10.5194/acp-15-6407-2015

Articles | Volume 15, issue 11

https://doi.org/10.5194/acp-15-6407-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-15-6407-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 15, issue 11

Research article

|

12 Jun 2015

Research article |

| 12 Jun 2015

Aerosols over continental Portugal (1978–1993): their sources and an impact on the regional climate

A. L. Morozova and I. A. Mironova

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Dec 2014	57	68	6	131
Jan 2015	20	19	6	45
Feb 2015	15	13	17	45
Mar 2015	21	3	5	29
Apr 2015	33	1	1	35
May 2015	14	5	3	22
Jun 2015	100	63	8	171
Jul 2015	34	21	3	58
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Oct 2015	26	9	0	35
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Jan 2016	28	13	3	44
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Apr 2016	4	2	0	6
May 2016	6	3	1	10
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Jan 2024	40	1	1	42
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Cumulative views and downloads (calculated since 09 Dec 2014)

Month	HTML	PDF	XML	Total
Dec 2014	57	68	6	131
Jan 2015	20	19	6	45
Feb 2015	15	13	17	45
Mar 2015	21	3	5	29
Apr 2015	33	1	1	35
May 2015	14	5	3	22
Jun 2015	100	63	8	171
Jul 2015	34	21	3	58
Aug 2015	14	14	1	29
Sep 2015	8	7	0	15
Oct 2015	26	9	0	35
Nov 2015	29	23	5	57
Dec 2015	9	14	2	25
Jan 2016	28	13	3	44
Feb 2016	22	5	1	28
Mar 2016	16	6	0	22
Apr 2016	4	2	0	6
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Jun 2023	32	1	1	34
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Feb 2024	35	6	0	41
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Short summary

The aerosols sources (volcanoes, mineral dust, wildfires, pollution) in continental Portugal were studied using ground and satellite measurements. The influence of the each source changes with the season and environment. Concerning the effect that aerosols have over the local climate variations change, the strongest influence was found for the less urbanized site and for the summer months. It consists in dependence of the maximum daily temperature variations on the absorbing aerosol content.

Aerosols over continental Portugal (1978–1993): their sources and an impact on the regional climate

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